Email this article A postseismic process in the area of the Simushir 11/2006 Earthquake recovered by the GRACE data
- Authors: Mikhailov V.O.1,2, Timoshkina E.P.1, Diament M.2
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Affiliations:
- Schmidt Institute of Physics of the Earth
- Institut de Physique du Globe de Paris
- Issue: Vol 471, No 1 (2016)
- Pages: 1188-1192
- Section: Geophysics
- URL: https://journals.rcsi.science/1028-334X/article/view/189122
- DOI: https://doi.org/10.1134/S1028334X16110179
- ID: 189122
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Abstract
The GRACE data make it possible to detect the areas where the earthquakes initiate postseismic creep in regions much larger than the focal area. This information is important for estimation of the seismic potential and position of the locked segments in the subduction zones.
About the authors
V. O. Mikhailov
Schmidt Institute of Physics of the Earth; Institut de Physique du Globe de Paris
Author for correspondence.
Email: mikh@ifz.ru
Russian Federation, ul. Bolshaya Gruzinskaya 10, Moscow, 123995; Paris
E. P. Timoshkina
Schmidt Institute of Physics of the Earth
Email: mikh@ifz.ru
Russian Federation, ul. Bolshaya Gruzinskaya 10, Moscow, 123995
M. Diament
Institut de Physique du Globe de Paris
Email: mikh@ifz.ru
France, Paris
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